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-- Database: `cw_61046`
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-- Table structure for table `AdminGlossary`
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CREATE TABLE IF NOT EXISTS `AdminGlossary` (
  `Term` text NOT NULL,
  `Definition` text NOT NULL
) ENGINE=InnoDB DEFAULT CHARSET=latin1;

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-- Dumping data for table `AdminGlossary`
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INSERT INTO `AdminGlossary` (`Term`, `Definition`) VALUES
('Acid-sulfate soils', 'highly acidic soils (pH usually < 3.5) that derive their acidity from the presence of acid-forming minerals (e.g., sulfur compounds), rather than from simple exchange acidity; oxidation of the sulfur compounds (e.g., upon exposure to air and drying) produces sulfuric acid.'),
('Af climate (K?ppen system)', 'climatic regime in which the average temperature of the coldest month of the year is 18?C or higher (A) and in which every month has 60 or more mm of precipitation (f).'),
('Am climate (K?ppen system)', 'climatic regime in which the average temperature of the coldest month of the year is 18?C or higher (A) and which has a short dry season; precipitation in the driest month is less than 60 mm, but equal to or greater than 10 - (annual rainfall in cm/25) (m).'),
('Ar climate (Trewartha system)', 'tropical wet climate, with not more than two dry months.'),
('Aw climate (K?ppen system)', 'climatic regime in which there are well-defined wet and dry seasons (''tropical wet-and-dry'' climate); the average temperature of the coldest month of the year is 18?C or higher (A) and in which there is a well-defined dry season during the winter, with precipitation during the driest month less than 10 - (annual rainfall in cm/25) (w).'),
('Aw climate (Trewartha system)', 'tropical wet-and-dry climate, high-sun wet season and low-sun dry season.'),
('Base Saturation (also sometimes referred to as Base Saturation Percentage)', 'the portion (percentage) of the cation exchange capacity of a soil that is occupied by basic cations; the remainder is occupied by acidic cations, and is referred to as the ''base unsaturation.'''),
('Base Unsaturation', 'the portion (percentage) of the cation exchange capacity of a soil that is occupied by acidic cations; the remainder is occupied by basic cations, and is referred to as the ''base saturation.'''),
('BWh climate (Trewartha system)', 'Dry, desert climate; hot, tropical-subtropical, and constantly dry. Potential evaporation exceeds precipitation, and the average annual temperature is not less than 18?C.'),
('Cation Exchange Capacity (CEC)', 'the capacity of a soil to adsorb cations; cations are adsorbed at exchange sites, and can be released in exchange for other cations.'),
('Chinese carp', 'any of several cyprinid (family Cyprinidae) fishes originating from China, including the ''grass carp'' (Ctenopharyngodon idella), ''silver carp'' (Hypophthalmichthys molotrix), and ''bighead carp'' (Aristichthys nobilis).'),
('Common carp', 'the species Cyprinus carpio'),
('Companion site', 'a secondary research site of the CRSP in a given geographic region; a limited program of research is supported by periodic visits by the US researcher stationed at a prime site.'),
('Csb climate (K?ppen system)', 'climatic regime in which the average temperature of the coldest month is below 18?C and above -3?C; at least three times as much precipitation in a winter month as in a summer month; precipitation in driest summer month is less than 40 mm; no month has a temperature of over 22?C, but at least 4 months are over 10?C.'),
('GAw climate (K?ppen-Trewartha system)', 'Aw climate modified by effects of higher elevation (i.e., cooler temperatures) in low hills or mountains. In the case of high mountains, the modifier H is used instead of the G.'),
('Guapote tigre', 'the species Cichlasoma managuense.'),
('Inceptisols', 'In the Soil Taxonomy classification, soils in humid regions that are as yet poorly developed, e.g., with little accumulation of clay or iron or aluminum oxides; a cambric horizon (a subsurface layer that has been changed by physical movement or chemical reactions) is often present.'),
('K?ppen classification for climate', 'The most commonly used system of classification of climates world wide, based primarily on temperature and precipitation regimes; published first in 1901, the most commonly referred-to version, including maps, is the publication Grundriss der Klimakunde, published in Berlin in 1931.'),
('K?ppen-Trewartha classification', 'Climatic classification system modified from the K?ppen and Trewartha systems, as described by Willy Rudloff in World Climates, with tables of climatic data and practical suggestions, 1981.'),
('Lateritic soils', 'tropical soils that contain a subsurface layer that is rich in iron and that becomes very hard upon exposure and drying and will not soften when re-wetted; the presence of iron often lends a distinctive red color to the soil.'),
('Marais', 'swampy, moist valley floors and river flood plains (Rwanda).'),
('Prime site', 'the primary research site of the CRSP in a given geographic region; a full-time US researcher is stationed at each prime site, and a full research program is carried out at the site.'),
('SMP lime requirement method', 'a laboratory buffer method for estimating the lime requirement of agricultural soils; this method is commonly used in many parts of the United States, and has sometimes been used for aquaculture ponds.'),
('Tambaqu', 'the species Colossoma macropomum'),
('Tilapia', 'may include any of several species in the genus Oreochromis, the genus Sarotherodon, or the genus Tilapia; in PD/A CRSP usage, ''tilapia'' most commonly refers to the species Oreochromis niloticus (sometimes also classified as Tilapia nilotica).'),
('Trewartha classification for climate', 'a modification of the K?ppen classification system by Glenn Trewartha (most recent publication is An Introduction to Climate, fifth edition, by Glenn Trewartha and Lyle Horn); like K?ppen the system, this system is based mainly on temperature and precipitation patterns.'),
('Ultisols', 'In the Soil Taxonomy classification, soils that have subsurface accumulations of clay but are low in bases (low base saturation); usually moist, but some are dry some of the time during the warm season; often high in 1:1 clay minerals such as kaolinite.');
